Geochemical characteristics of the La Réunion mantle plume source inferred from olivine-hosted melt inclusions from the adventive cones of Piton de la Fournaise volcano (La Réunion Island)
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DOI: 10.1007/s00410-017-1397-2
Abstract: Major and trace element compositions were obtained for bulk rocks and melt inclusions hosted in olivine crystals (Fo > 85) from the adventive cones of the Piton de La Fournaise volcano (La Réunion Island). Ratios of highly… read more here.
Keywords: adventive cones; mantle; melt inclusions; trace ... See more keywords